Quaternary neotectonic configuration of the southwestern Peloponnese, Greece, based on luminescence ages of marine terraces

Επιστημονική δημοσίευση - Άρθρο Περιοδικού uoadl:3070298 17 Αναγνώσεις

Μονάδα:
Ερευνητικό υλικό ΕΚΠΑ
Τίτλος:
Quaternary neotectonic configuration of the southwestern Peloponnese, Greece, based on luminescence ages of marine terraces
Γλώσσες Τεκμηρίου:
Αγγλικά
Περίληψη:
This project studies marine terraces in western Messenia, southwestern Peloponnese, Greece, to propose a model of neotectonic configuration and paleogeographic evolution of western Messenia during the Quaternary. GIS analysis of topographic data and geological mapping revealed flanks of raised terraces created on Quaternary marine deposits. Luminescence ages of sediments from the three westernmost marine terraces tend to be consistent OIS-5, OIS-7 and OIS-9, respectively, thus agreeing with the three latest warm stages of the Pleistocene. Moreover, the type and the extent of deformation of the dated marine terraces allowed us to reflect on the neotectonic configuration of western Messenia as well as to conclude that progressive differential uplift over the last 300 ka has induced a dome-like structure to the upper crust of western Messenia. © 2013 China University of Geosciences and Springer-Verlag Berlin Heidelberg.
Έτος δημοσίευσης:
2013
Συγγραφείς:
Athanassas, C.
Fountoulis, I.
Περιοδικό:
JOURNAL OF EARTH SCIENCES
Τόμος:
24
Αριθμός / τεύχος:
3
Σελίδες:
410-427
Λέξεις-κλειδιά:
deformation; GIS; luminescence dating; marine environment; neotectonics; Pleistocene; Quaternary; sea level change; tectonic structure; terrace; uplift; upper crust, Greece; Peloponnese
Επίσημο URL (Εκδότης):
DOI:
10.1007/s12583-013-0334-1
Το ψηφιακό υλικό του τεκμηρίου δεν είναι διαθέσιμο.